A revision of Ophidiaster davidsoni de Loriol and Pellat 1874 from the Tithonian of Boulogne (France) and its transfer from the Valvatacea to the new forcipulatacean genus Psammaster gen. nov.
{"title":"A revision of Ophidiaster davidsoni de Loriol and Pellat 1874 from the Tithonian of Boulogne (France) and its transfer from the Valvatacea to the new forcipulatacean genus Psammaster gen. nov.","authors":"M. Fau, L. Villier, T. Ewin, A. Gale","doi":"10.5194/fr-23-141-2020","DOIUrl":null,"url":null,"abstract":"Abstract. Forcipulatacea is one of the three major groups of extant\nsea stars (Asteroidea: Echinodermata), composed of 400 extant species, but\nonly known from fewer than 25 fossil species. Despite unequivocal members\nbeing recognized in the early Jurassic, the evolutionary history of this\ngroup is still the subject of debate. Thus, the identification of any new\nfossil representatives is significant. We here reappraise Ophidiaster davidsoni de Loriol and\nPellat 1874 from the Tithonian of Boulogne, France, which was assigned to\nanother major extant group, the Valvatacea, and reassign it within a new\nforcipulatacean genus, Psammaster gen. nov. Psammaster davidsoni gen. nov. possess key Forcipulatacea\nsynapomorphies including compressed ambulacrals and adambulacrals and\ntypical organization of the body wall and arm ossicles. A phylogenetic\nanalysis including Psammaster davidsoni gen. nov. does not place it within any existing\nforcipulatacean family. Instead, Psammaster davidsoni gen. nov. exhibits a mix of plesiomorphic\nand derived characters and is resolved as a sister clade to a large group\nincluding the Asteriidae, Stichasteridae, and Heliasteridae. Removal of this\nspecies from the Ophidiasteridae means their oldest fossil representative\nnow dates from the Santonian, Upper Cretaceous.","PeriodicalId":48830,"journal":{"name":"Fossil Record","volume":"23 1","pages":"141-149"},"PeriodicalIF":1.9000,"publicationDate":"2020-07-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Fossil Record","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5194/fr-23-141-2020","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
引用次数: 0
Abstract
Abstract. Forcipulatacea is one of the three major groups of extant
sea stars (Asteroidea: Echinodermata), composed of 400 extant species, but
only known from fewer than 25 fossil species. Despite unequivocal members
being recognized in the early Jurassic, the evolutionary history of this
group is still the subject of debate. Thus, the identification of any new
fossil representatives is significant. We here reappraise Ophidiaster davidsoni de Loriol and
Pellat 1874 from the Tithonian of Boulogne, France, which was assigned to
another major extant group, the Valvatacea, and reassign it within a new
forcipulatacean genus, Psammaster gen. nov. Psammaster davidsoni gen. nov. possess key Forcipulatacea
synapomorphies including compressed ambulacrals and adambulacrals and
typical organization of the body wall and arm ossicles. A phylogenetic
analysis including Psammaster davidsoni gen. nov. does not place it within any existing
forcipulatacean family. Instead, Psammaster davidsoni gen. nov. exhibits a mix of plesiomorphic
and derived characters and is resolved as a sister clade to a large group
including the Asteriidae, Stichasteridae, and Heliasteridae. Removal of this
species from the Ophidiasteridae means their oldest fossil representative
now dates from the Santonian, Upper Cretaceous.
期刊介绍:
Fossil Record (FR) is the palaeontological journal of the Museum für Naturkunde Berlin. This journal was founded in 1998 under the name Mitteilungen aus dem Museum für Naturkunde Berlin, Geowissenschaftliche Reihe and appears with two issues each year. Fossil Record publishes original papers in all areas of palaeontology including the taxonomy and systematics of fossil organisms, biostratigraphy, palaeoecology, and evolution. All taxonomic groups are treated, including invertebrates, microfossils, plants, and vertebrates.